Number of the records: 1
Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)
- 1.
SYSNO ASEP 0330111 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe) Author(s) Rajchl, M. (CZ)
Uličný, David (GFU-E) ORCID, RID
Grygar, R. (CZ)
Mach, K. (CZ)Source Title Basin Research - ISSN 0950-091X
Roč. 21, č. 3 (2009), s. 269-294Number of pages 26 s. Language eng - English Country GB - United Kingdom Keywords Cenozoic Most Basin ; continental rift ; Eger Graben Subject RIV DB - Geology ; Mineralogy R&D Projects IAA3012705 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) GA205/01/0629 GA ČR - Czech Science Foundation (CSF) GA205/06/1823 GA ČR - Czech Science Foundation (CSF) CEZ AV0Z30120515 - GFU-E (2005-2011) UT WOS 000266171900001 DOI 10.1111/j.1365-2117.2008.00393.x Annotation The Oligo-Miocene Most Basin is the largest preserved sedimentary basin within the Eger Graben, the easternmost part of the European Cenozoic Rift System (ECRIS). The basin is interpreted as a part of an incipient rift system that underwent two distinct phases of extension. The first phase, characterised by NNE–SSW- to N–S-oriented horizontal extension between the end of Eocene and early Miocene, was oblique to the rift axis and caused evolution of a fault system characterised by en-échelon-arranged E–W (ENE–WSW) faults. These faults defined a number of small, shallow initial depocentres of very small subsidence rates that gradually merged during the growth and linkage of the normal fault segments. Workplace Geophysical Institute Contact Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028 Year of Publishing 2010
Number of the records: 1